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本文根据在117°～135°E,21°50′～41°30′N范围内的500多个热流值,对中国东部海域及周边的热流分布特征及其与地质构造的关系进行了讨论。热流分析表明,冲绳海槽具有极高的热流值,为一现在正在活动的弧后张裂带。
Based on more than 500 heat flow values in the range of 117 ° -135 ° E, 21 ° 50 ° -41 ° 30’N, the distribution of heat flux in the sea area and its vicinity in eastern China and its relationship with geological structure are discussed. The heat flux analysis shows that the Okinawa Trough has a very high heat flow value and is now an active post-arc episode.